Field notes, Kentucky Geological Survey, undated

KENTUCKY

Kentucky Geological Survey. Lexington, Ky. If found, please return to Aug. F. Foerste 1017 Grand Ave. Dayton, O. Will pay $1.00 for this favor. Finished

5 40. Devonian worm br. l. sand. fish tails MH Hisle (3) 5. 1/4 mile South of Indian Fields 18" Solid greenish Dev. limestone 12" Fish tooth layer, 0 2 1/2° Bridge up to top of Cezgord 38{ 15 1/2" Base of clay, to bridge, up, Clayey limestone Hard limestone with Hyellia, etc. at a former time I found here Halysites catenulatus Streptelasma large 40. N of John Giff 25-0 yds. Base of Wavely Clay, / 1110° 40° Black Shale Traces of phosphatic rock 12" clayey Clayey layers in 6" 8" clayey Black Shale, E of G. Bearfoot lime, m James Catledge farm. 38° 8 1/2" Lucke level up to clayey layer. Base of Black Shale. 1027° 10m 18" Sandy rock with worm borings, clayey beds 6° 2" 22" Limestone 18" Sandy rotten stone 9° 11" Foraminifera and l. Fish plate 38° 5" Fish layer. Top of Cezgord Wauswabi at MH Hisle locality, 72 limestone

41 Abbotts Mill belongs to Swope, 2 miles south of RR crossing over Sulbrend creek, 30" Top of Der. L. with worm burrs. 15" Devonian ferruginous L. ½ ft Orbulary First obole. 19" White clay. 1/2 Ferruginous limestone. 11" White clay 2 3/2 ft Clay with ferruginous limestone layers at various levels. 3ft 4 in. Ferruginous limestone, Partly by alor chint m. 3" Zaphrentis Danf ammon's lay Zaphrentis calyculs Rimicopora frindosa 3 ft 7 in. Ferruginous Chint m. blue clay, at base , at Abbotts Mill, Cyclinema clint meneri, Leptaeia rhomboidalis. Clatherpura frindosa 2ft soft clay shale. 5 sluiced. Base of Black Shale strongly Devonian ironwall in section. 27 1/2 ft up to Derwian. 60' 9 1/2 ft Clay with L. layer at top 25 ft of creek level at grad cross- ing to top of usual lime- stone rubble on grad bed, limestone layer at top. Includes much clay in section

1/2 mi. S. of Moberly. 12 1/2' solid Devonian limestone 5 1/2' clayey limestone, weathered black, little exposed, Dervm, osgood white clay, 25' Limestone w/ its interbedded clays. 17' Lower Osgood large crin. heads, Whitfieldella. or this flabellus, Stupellaria 13 3/4' Clinton. Photo No 3, 4, store at Roslyn Station Belno dam or river, Section at Mansfield Mill, at Roslyn Station Cat Creek Mouth, more clay on top not studied, water worn. 2' from Moberly source, evidently fragments of rock apparently layer composed thin frag- 29' slightly firmish. variable in texture some parts Whiteish clay 6 1/2' sandy near base, (sub- Carboniferous chert) rounded, freestone, quartz + 20 9" firm by iron, angular crud River gravel, Pebbles stained light concretions rare, one at top of section ferruginous layers, phosphatic small fragments, in the local 90 9" soft blue clay shale, crackling into Red River.

From R.R station at Stanton, 1/3 mi. N on main road, and 100 yds east. Black shale, top, contact with base of Waverly, along E+W road. Judge Hardinick's place. 72. Half a mile west of Shawnee station at western corner of Clay city, 4ft ferruginous limestone with crude chert. 1ft soft weathering rock, with snails (Chenoplychina) in lower part, 20ft ferruginous limestone which ferruginous limestone with black nodules and fish remains in lower part. Near top of bezora clay with thin layer of clayey rock with vertical worm borings With 2 feet of top of bezora ocon Favrites favosus and several cyathophylla crass, In 20 in layer spirifer franklini. 43. According to John Grif at Tipton's Ferry, Devonian limestone occurs almost 20 feet above level of river, 1/2 miles SW of Clay city. 44. At mile post 30 miles from Lexington, Heterisangia, gastropoda, lamellibranch, and Platystrophia sili sandy and clayey beds at top. Platystrophelia + Bryozoans in their beds beneath. 45. Tom Wilkibbot about 1/4 mi. E of 30 mile post. Just east of linee along railroad is first exposure of Platystrophelia lynx. Below which across cornfield is spring. Platystrophelia lyncx here also at stream level. Three fine thick section with Platystraphelia lynx. 46. Clint on at top of six exposures. Consider- able Bidium m K exposure in cut Strophaneura silcata canum, Helotella serrata with dorsal sines, as in madamme called accidentals. Platystrophia tipinata. Ropiniqquina altuneta set line only, Streptclasma rusticum spicatum Streptclasma divaricatus common Pterinea demissa noval, size

Residual Der. l. + Black Shale. 47 10'28 ft whitish clay. 41½ 13½ ft ferryl clay, ferruginous layers? ½ ft ferryl l. full of Cyathiphyllum 4½ 2ft clay? 2½ ft ferryl l. in thinner slab with clay below 7½ ft fairly continuous ferrug from limestone, small crinoid beads and small Cyathiphyll at top, A. 7½ Locality: at west end of Co grand clay dig. gings near for Talladega R.R. almost 4 mm W. of Indian Fields. Base of section at level of stream crossed by R.R. 48 West of crossing over Howard Creek. of l. in clay at this level than elsewhere, well exposed. This is a thicker section tinged with deep red, a purple red; 5 ft thin light brown l. with layers at 44. 18½ ft lower part with limestone m.s. A 7ft ferruginous accret l. crinoid trace small. Section 47 White clay chiefly 28/ft measured 41½ ft chiefly clay Probably chiefly clay with the l. 6' layers at top 13½ ferruginous layers, fairly 4½0 thick, with clay latera more massive l. 7½ Bed A Slope of rock 2.8 ft in 100 ft, Section 11 48 2.8 5/7 19.6 23 42ft clay estimated according to dip of 2.8 ft per 100ft. white red purple tinge 5 ft thin l. + clay cruffy cray with l. at diff. 18½ ft levels, especially not thin 4 ft if trace. more limestone 7ft

49. Section. with thin clay partings. 8ft, chiefly light brown l. iron brown valo. if limnet one at irregular inter m of per 1 ft. and then others 5ft of stiff clay chiefly with limestone wave marked at top the limestone is straugh 7ft Ferrying one with clay between 5½ft Ferryng, l. with clay between y dents of Gyathrophyllum at top Ferryng, massive, b. C B 12½ ft. B clay readings A. Fossils in B. -Calyxnum vagdent. Gyalophyllum elegula -Phyllodendra angulata, -Rhyndimilla calhouna. -Rhyndimella funidra. -Dalmabella elegantula, -Cyclameria Daytenuis; spp. -Gattglyphum Daytannus large; -Thyphelia Ormest, large spines; -Orbis fissiphica = Orbis stult? -Phaceros expansa andae form Septaria sliuvidalis -large erinoid beads. (13 Layer D 8 ft chiefly l. with clay partings. 25½ ft x. Layer C 5ft clueit caly, a little l. at top, Wavy layer. Layer B 12½ chiefly l. with clay partings. 7 Layer A Mississip 51 ft Richmond including Rafinesquiana at base, chiefly breathering is small clay and clay aments.

(15)

Section 49 continued. (Remembering at bug of 51ft.) 51 ft. Richmond, clay rock weathered by to small fragments, 30 ft. Well bedded clay rock, my cover 15 feet well exposed at cut just west of mile post 31 By Lexington. 11 ft down farm road to north 1 ft heavy fossiliferous Rock. 50 ft to top of Lynx beds. There are chasms along Howard track and always becoming just east of Mr. Jims Horn back to time. Lynx beds See second page preceding. 6 S. of J.T. Elkins, along Rm. (17) Fissile Black Shale above. 30" Black Shale layer in clay rock--trace? 3 3/4" Cherty Criniferous 1 3/4" unknown. 1" solid brown limestone, origin? 12" blue clay 30" 2"-4" to lime cl. 29 1/2" 5" chiefly clay 24 1/2" 4"-6" solid brown cl. 24 1/2" 8" 2" clay 16" 2" clayey limestone. 16" 5 1/2" chiefly clay, some limestone, 1 ft above line. 10'6" From Clinton layer to top of cave continuous exposure. Farther south, at lowest point of road, the base of the Clinton is clearly shown resting on clay shale. Clinton or layer with large crinoid heads = 14 1/2 feet. The layer in which the heads occur disintegrates readily, as do also other layers above the middle. The lower 6 1/2 - 8 1/2 feet are quite solid. The layer takes as base of bog sand is quite solid, or was bedded = 6 in. Where cl., up to 2 feet. 6 ft blue shale mixed with small limestone pebbles. 6 in limestone. about 33 ft to Corniferous

8. Road going East of Log Lick Church. {3° 4° 1° 65° brecciated layer cherty Corny. bram [red] limest m., B ozre f Clint m to face of Cornf, 7. Met. J James Stones home. 80° from Red river to Clinton. 5° brecciated layers. 6° chert streaks + chert nodules in all parts. 85° Clay with some limestone layers especially near the base. Contact not clear. 8" heavily bed. massive cross- budded. [illegible] base. 3 ft mullen mm clayey near top at least, rest probably rotten l. 2 ft. limnest clayey weathering much. 8 ft. solid Clinton. 80 ft. Red river to Clint m. 9. On road leaning jike 1/2 mi. S. of Indian Fields, At Browlgx Bruner's home Is this from limestone? [illegible] 15 ft to tops of D limest m. 1 yd solid limest. bram (39ft) 22 ft cement. 13" limnest, several layers, 12 ft clay 6" solid limnest. 8" clay 22" limestone asqted? clay layer soft.

(21 Section 50 Section 50, Across from Vienna, along road to Old Jones Furnell. 5 ft 3 in. Hard brown limestone, firm 1 ft Brecciated, 1 ft Soft rocks 6 ft Crumblers no much clast, Contact not exposed. { feet per 100 feet tracted at rate of rise of 2.8 (2 ft) 75 ft measured 13 ft out { also below Sand possibly firm limestone 6 ft Firm exposed, limestone at top 5 1/2 ft thin firm limestone, 6 1/2 ft not exposed, probably chiefly clay thin, clay part way 3 1/4 ft partly exposed limestone Scather thick down this to play { layer of limestone, clay centary 9 1/2 ft (to top) strongly cross bedded - 4 ft 2 in. Marbles chert m. 4 8 ft to face J. Clinton 14 3/4 ft well bedded clay limestone 17 1/2 ft below, road to face of well bedded clay limestone Section 49 clay wavy mudstone marble firm exposed firm limestone, partly exposed partly exposed strongly cross bedded marble

Section 51 and 52 of Niagara suggesting faulting. Section 52. N side of hill - opposite side from section 51. 3 & ½ ft from top of last to top of this in next section. 162 ft from plane from line steps with mud clay herein went down full 60 feet without seeing anything but limestone. Section 51. From Vienna north sign of Devonian seen, top of exposed but not 123 ft above base of Clinton to (Favorita favons very large where I structure claim, also Hindieophlebidalis from 85 ft above base of Clinton so clay, but cutting pattern found no one should with exposure shows limestone base, practically correct. 30 ft from supposed Clinton Archimeda top? 12 mi. NE of Vienna, Section 53. At junction of ridge roads, Devil. Black shale above, 67 ft. Clinton base to base of Devil 44 mi. S. of Dry Lick Church Section 8. Dry Lick Church. 2 ft Associated layer (Black shale) 4ft 5 in massive cherty (but soft at base) 9 in solid. 66 ft from base of Clinton to Dev. section 6. 33 ft base of Clinton to Stucklan dinia layer. Section 4 Old Billy Snowdon farm, 62 ft. base of Clinton to base of Corniferous. At head of Drong Branch. East of branch from Morgan Cembarkes farm is struck. Candinia at same level as at section 6 = about 30 feet up. 1/2 3 1/2 ft high

(25) 55 at crossing of road N of RR bridge 4 ft 8 in. Devonian l. total. E of Marneetown W side of Day City.) 43. Tuttle's Ferry on Red River, SW of Black Shale Clay City, 4ft 8

(27) 59 At crossing near Dullespond Sand S of Affett's Mill. 73 ft to face of Clinton Crown Ford 60 East of Aries, in road from Plymouth to Merritts, Including the lower layers again left to the precicated is total the clays. - The D formation is 5ft. The lower 18 inches found with very little clay, most of the angle looks like bed which elsewhere is preccrated. Near Groozeyold Stand Mill Bridge. Photo 6. W of Aries, east of Dc on asphal Roadway Clay on Black shale base Near old Simpson Brook place. 61 At the junction 2 mi. N of Merritts, limestone partly exposed; clays, corresponding to Fort Clay. 1½ ft. Clinton strata: in middle: Calculus, Dalichnellus distinctus. Phacops, etc. in dark grey sand beds. Stands on right of road and 2andy in white clay; also black Fault bringing all of Clinton nearly up to D overlie by stone. Cyclopis (?) sandstone, very Abrev below boundary and river to top of lamelli- cient clays and some olive Petr adim thin layer, poles, chiefly lilsin tiff 30-35 ft Somewhere thin fibrium layer, nrad at turne is a line above the level, in 5 ft clay shale, sand, larger at top, about (probably 14) o of Clinton m. west joint in road at tunnel. by few. my rock layer. Limestone joy shale with chindware layer on brick weather slightly, + by grey sands very dense- la strataa, lnygamous, quina frondum, Oltus lynx, branches, abundant letters; river to hard layer of ledge at expense. bosome clayy shale + not so but maybe 2 feet start in dant points. at top = Cathred ells bands. - 4 = 165 ft lamelli to Clinton 1½/19 3-2 - by top to Clinton

Merrih

59 At crossing over Lulbegrand Road 5 of Abbotts Mill. 73 ft to face of Clinton Grove Ford 60 East of Aiken, on road from Pittsgoule to Merritt, Including the barren layer again. Next to the brecciated is total stricture. 1 The D formation is 5ft. The lower 18 inches formed with very little shert, most of the angle looks like red which elsewhere is brecciated, near Gorseyfield stand Mill filled. Part o-5. W. of Aiken, east of DC on an emb. Residual clay on chalky shale try near old Simpson Creek place. 61 Pike junction 2 am't to Merritt, limestone partly exposed; slags, corresponding to soft clayly 11½ ft. Clinton The in the bottom Calycula Dalmanella etc. numtous Pholadomya fuscastra are worn beads. It andy crevice bed any 2 sandy sh. of fine grit and brick. Fault bringing about 20 feet up nearly up to D or lower clay and stone, by the junction channel; 62. Merritts Ferry above Beland landing in much red 4 ft above river to top of Lamelli- larger a slent drift area Streptilacema abne Tetradinum Tetradium layer, are found, chiefly felon 20-35 ft chief 30-35 ft Somoyeose Tetradium filatum layer. 35 ft above road at turn is Limestone line about river level. broken in 5ft clay shale Grasse sand, larger at top, 12 ft Clinton about (probably 14) 125 ft to face of Clinton m. 44 ft rise to highest point in road at turn; and lynx few, 12m red clay rocky layer & Stromata 6½ft soft clayey shale 3 in. Lobelia? chondratis layer cm grist brick weather snuthly, 11ft Ph. lynx + Snyz sps very abund- Strobilula signata Saygzaus. 6 in. A sphygina fordani (Litho) lynx, 12m Lamelli branch, abundant Lettere. ½ ft 2 in. from river to head layer forming top of ledge at expense. front & exosome clayey shale + not less informs but upper 2 feet start in river abundant fossils at top = both are red & Lamelli bands do. 44+125=169-4=165 ft Lamelli to Clinton -14/15 3½ = Lynx top to Clinton

63 [illegible] 120 feet top of Lynx hds to bottom of Clinton in direct measur ment, on east side of creek where rocks dip east about 7 ft 4 in. in 65 steps 155 ft is probably erroneous near crest, inclining allm once in a lb of angles. Clinton in Whitfieldella. The calculations for dip gave 180 feet but this seems absurd, 2. Hollywood at Smith Mill. Black Shale, 20 in. Brecciated rock. 2 ft 3 in. Dev. Limestone. 21 in. candy rock, nodules + fish remains 4 ft 4 in. Irish limestone, solid forming falls, gray clay beneath. 64 White Oak creek road at Erwine, W of road 1/2 mi S of junction of White Oak road and road to Callaway creek, Black Shale, Devonian cherty l. 52 1/2 white clay part of this section grey in color 11 ft white clay with hard flint shale in 1/2 foot thin brown limestone, 5 1/2 ft white clay C 2 ft solid brownish limestone, 25 ft white clay 5 1/2 ft ripple limestone thin layers 24 qft not exposed stream branch. 126 ft = total of above section From C down to top of limestone layers at top of Clinton equals 44 yd at forks of White Oak creek one and road to Callaway creek, 78 ft to top of Dev. L. This measur- ment is quite accurate. The thickness of the Devonian limestone such as at least 75 ft but must be measured near the river, while the exposures are later at base of section. Other fossils: Plectamphorus trainsorals, orthus descendula, Phinupena pladna, Sep. Tamarachnoides, Pizzenariola, Calymene megacephala, large size.

66. West J Rice Station m and clay layers, at least 40 ft Great thickening Black shale above 4 ft thin clay dark brown black shale 2'2" clay [illegible] 24" inches solid clay, l. [illegible] 18" shale smelly of sulphur very grey. 16 in solid l. wet chert firm - flocculent. 20 ft Coniferous with chert 20-22 ft [illegible] Gypsum hard as that it is difficult to drill line. This Coniferous section is thickened perfectly from 7 or 10 feet only to ground chert) 65, 1/2 off way between R R station R R bridge at Davis; 4" Black shale by 6 ft? [illegible] layers clay rock in bar 6'ft 6in, Cherty Dark, next met a canyon at top. 8 in dark sand with Ambrosella + [illegible] layer at base) with 3 in layer dark sandy fish 3 ft 3 in Massive very firm l. [illegible] 67. E W of tunnel 1. Black shale with alum salts at base, 10ft clay layers in Black shale layers 19ft Black shale, clay layers above The preceding sect is [illegible] it should supercede was no estimate in this sec- Black Shale. Since then 18 1/2 ft's fromiferous layer base in sedims. 4 ft hard rock associated with other 16 ft strongly Cherty Dark, 2" Blue clay with 1" firm grayish blue chert [illegible] clay

68. Above find depend to right of Big Doe creek Black shale & exposed down to river's edge, Newman b. exposed new bread waters of creek. 69 No exposures of Beograd bed near or above Station Camp creek. On road here no Derriman thicker than 7 feet seen north of Station. Camp creek but exposures are poor = Between Station Camp & Blue Bank. 70. At Miles Creek, well begun 10 feet above RR, strike sands rock over Doer, accord ing to driller, at 145 ft and cliffed at 605 feet at another gap went shallower will at ford. 68 was 96 feet deep, red d and actually at top sandy layers over Derriman, 605 145 462 162 280 Fossils in upper front of (33) Chinon, Muttfieldella yoni, Stenillasma culcyana, Rhynchopora fruticosa, large rigid head, Zemantilla elegans,ulus, Yaptaria rhomboidea, Algyrotheca a colina Clibostromites nanus, echis Calymene vorodesh, Prasophora chinan mexica, 12. Platystrophia lynx oblyt puer polle uae. Cyclhem don't remember. 280-282, Parade to Braesfield, Black Shale. 5 ft. grey Derriman shales. Clay, 57 18 ft not exposed well, chiefly with sand clay 39 6½ ft thick, 1 thin shale interbedded thin clay. 2 ft more interbedded with 3 ft 9 in. Sandstone & thin lime

(35 71. - at Braasfield Black Shale. 1/2 ft brecciated 4 " same fossils over chert 1/2 ft bluish stone earthy " Oozed clay, Blue Clay - is seen in R&R cut nearby, this part 8 inches over depth of preceding section. 72. 10:00 NE of Irvine, 56 1/4 ft No exposure except at top: foot 56 ft Merthyr & Cardiff shales, in tuffs Shear but some in artesian sample. then a sandstone of fragments of 210 ft Chazy gray below up to 100 ft Glabic nodular layer 7 ft rock, grey clay shale same phm 49 ft Hard clay with bit above + bit at the 2 & 1/2 ft red. Clay from stone at top. 11 1/2 at top is flinty clay weak layers gather in shaly Below very dirty or extra part at the top greyish clay 3 8 ft [illegible] clay nodules, some run 13 ft grey shale, iron stains at top, up to this level 5-1 inches thick 5ft. plinplate nodules scattered Shale 95/2 ft from road to top of Black Base of Black Shale not seen

279 - tellistai 1 ft 2 in sandy gray rock 1/2 ft gray rock massive rock, chance tand with remainder 20-24 in, from 4 ft reddy gray. well bedded, with 29 ft not exposed. 10 2 ft limestone layers at top; (The last layer: sandy layer.) (Four inches (rounded) with almu) large crinoid heads, whit fieldsh, 1/2 ft clayey limestone for upper 1/4th, at top; 3 3/4 ft thinly bedded. large crin'd head 7 ft solid bedded Clinton. 3 ft 6 in. solid massive Clinton. Clay rock (Richmond) bedded, Black Shale, 2 1/2 ft massive, = disassociated rock; 1 ft 2 in. in 3-4 in. layers, solid 1/2 ft 4 in sandy gray rock weathering 2 ft massive with crinoid stem 6 in nodular layers. 1/2 ft gray massive rock. Dermium 15 1/2 ft. 20 ft clay? 13 ft limest + clay; 5 1/4 clay 7-1/2 limestone, rem [illegible] 73 Lexington Tile Roof Co. Maco Shingle Tile, Thronton & Ross, McCullan Ho. 5 ft of clay overlies the Black shale at the shingle tile work; 6 in. I am not verifying this is stripped away. Clay dug, soak it, leave overnight for drain tile, brick, shingles. Next day clay is shovelled into the disintegrators. Then cray at me present if clay is crushed, fragments crushed down to 7/6 inch. Carried by belt from disintegrator to to the tile wheel. The clay is pushed out of the tile wheel through the chutes where the profile thickness and weight is given to bricks, shingles, &c. The clay pushed at to corners to cut off tails, where these objects are cut off to perfect lengths. Clay for shingle + anything I & dressed, is shaped up at least 2 days, cooked to oil cloth, to get evenly moist = winter temper. Can be kept all winter. Then it is pressed. Shingles, &c. In case of shingles the wheelhead is stationary, and there 3 clams dries plies are runnable after black shingle is prepared i,

lifted up together with the lower die and placed on a pallet, turned, and the die lifted off. Carried in pallet to dry shed. Capacity 4000 shingles in a day, 16 hours, for 1 small Let dry by air from 2 to 5 days depending on weather. They all shoved in the pallets. When dry they are sheathed (=trim) off along edges and corners) and stacked up. Taken to kiln, shingles set up in edges, 8 in. gap, and fire bricks bricks between. Fire day secured near the works. Burned 72 hours. Let not fresh smoke at top holes. This takes (39) almost 24 hours, no great heat used, Then have heat gradually to a white heat, which takes about 48 hours square, then clean down the heat just firing & close up the fire doors. Takes 3 days to cool, 1½ to empty, 1½ to fill. 3 men will fill the kiln or so to make 50 sq.square a day = 250 shingles to 1/2 square = 10ft x 10 feet surface of roof. 2 men at dismantling no. at mill = 1 cut of 1 man 2 off barriers, that wheel 4 dry the shingles. Burn off 25 dry blanks in a good stack, in this will only 15 sq.ft. stack in Bunk, back close. 1 man at leveling press. 1 feeder. 1 dumper 1 off barriers, to pass & away 1 skipper & trimmer. 2 off barriers to fill the kiln guid 1 to set it & stack up. 2 men to fire. 1 day on an 1 night man. $1.00 per day, except kiln heater who gets $1.50 perday because an expert. Compressed brick - Bryd. 2213 # 2.

(41) shingles- 650 pounds to a quar =100 sq feet, expense is 9 1/2 by 6 inches. Clay shrinks 7/8 in tr 1 ft., judge of temperature by clear. by a brick open oven each side in front of kiln. Pompey brick, 8 3/4 X 8 3/4 X 2 in. or 1 ft = by foot expense. Also made tiling & brick. Shingles made here about 2 years, Sanguis subspatula is taken Black shale, H. Mobley Tiling Manufact. turing Co. J Wilson Tate, We Little Wonder Press, made at Frankfort Indiana by Wallace Mfg. Co. turns out 5000 tiling & 2000 brick per day. Tile table called Earnings Automatic Clay Cutter. Mfd. by J.J. Fate Co. Plymouth, Mich. About 3 feet clay over black plate is used. Strip 3-4" Loan is $1.50 per day at 10 ct per hour Tile Truck wagon made by Arnold Creager Co. Newt London, Ohio. 30 horse power, for 4 inch tiling it takes great power. 8 lb-4-6 inches Takes about power for smaller size. Brickmaking Machinery ask Wallace Mfg. Co.

(43) 26½ ft not exposed. Partially sandy clay shale. 13 ft from gate top of clayey sand, exposed, IV fossils. 50 ft not exposed, partially sand clay shale, like specimens above? 1 ft dense limest. below 2 ft sandy shale with a few thin sth dense limest. bed layers 1½ dense blue limestone 5 ft I would like that called Gar dard 2 undet one... River. The dense limestones en- tain crinaceae, small gas trilobeds, large spines, all too possible to get out in excavation. Calam. section = 165½ ft. Calacaecia is erad. bed at top of well at level of dense formation 5 Colt Ferry, west if 9 ft fractured, clay and limestone Top; I want to close here, also some what near base typical. 6 ft very shifty, base not seen. 10½ ft clean forster calc. shale. 20 ft in lowest 3 layers. Base not seen. 14 ft Wst/nelida bed is fill of a large thin band of limestone. 2½ ft I understand the Whaffsela ella layer, before this new clayey west comes in topmost. 19½ ft beds thicker at base here. 5 in. White middle full for 34 parts, 3¾ ft irregular Clinton. 54 ft clay part of Richmond in the Lown well then traces of lime stone, apparently formed after depositing clay are formed in clay and recede some the clay in beds, a small limestone in certain parts. 9 ft from top of Whaffsela top clay l. Relative to strata at Calacaecia Streptoceras Streptoceras turn out small valves as parasitic. at base field in. Here also in turn is vertical valves? Strept. nevis retincta, 5 ft several specimens of streptolhoma at various levels.

76 J. & Cornelison and Son. Bybectown, Ky. = Portland. Clay is obtained on road from Waco to Cobb Ferry, about 1/2 m'l E of junction of Waco- Cobb Ferry road with pike thru Waco to Divine. Thickness in an average 6 or about 5 ft. The clay rests the Black Shale. Clay is brought to slimp and glazed as jugged, using one horse and tub. Taken from jug to cellar; Jars 1qt 1/2, 1, 2, 3, 4, 5, 6, 8, 10 gal. jugs 1qt 1/2, 1, 2, 3, 4, 5, 6, 8, 10 gal. Churns 2, 3, 4, 5, 6, & gallons. Blaze with slip clay get from New York, delivered to crime from Florida mixed with red lead and man garase. They is all stirred together the clay being strained first + then the pottery is dipped + dried, and then vt's to the Kiler. Used as down draft kiln, fuel: coal, heat up slowly for about 24 hours; and raise to white heat in 24. Leavers great hole, + use a try piece, where the clay is good on this try piece and it clues. Curl 50 hours, Tilings, 4, 6, & inch. 77 D. Zittel + S m. East end of Waco, Set clay in George McMinnys place, about 2 mi. SE. + 6 ft if clay overlying the Black Shale. In same place 4-7 ft clay is found on sand, in there cases the clay is counseled with them their resting on Black Slate. It will do and a little more fire. jugs. 1qt 1/2, 1, 2, 3, 4, 5 gal. jars. 1/2, 1, 2, 3, 4, 5, 6, & 10 gal, Pitcher, 1qt 1/2, 1, 2 gal. Churns. 2, 3, 4, 5, 6 gal with lid. Flower pot, 2, 3, 4, 5, 6, 7, 8, 10, 12, 14 nd Fruit jar. 1qt 1/2, 1 gallon with lid. Chambers, 1/2, 1 gallon. Fruit jars. 2, 3, 4, 5 gall. to put in has lid. Can be sealed. Used largely for storing corn + stuffin' jars, Milk pans 1/2, 1, 2 gallons

(47) See Albany slip clay, red lead and manganese. Albany, N.Y. Slip clay is obtained frm. Bover Pottery Co. Lumberville. 78 Velcro's Spring ½ Ton Curtis N 1 Falling Branch 1mi NE of Waco. 18 ft Cmp practically little sheet in Devil's, overlaid by 11½ ft earth shale, overlaid 2 3ft. massive earth rock. 13 ft eathy clay, 9 in the pure slate, and with casts also becoming black and fossil abor. 79 Clay pits used I man at Byke- town located ½ E of Waco, when lived across Falling Branch along the Waco - Coll Ferry road NW of said channel. 80 When road to Colb Ferry leaves the Big Easton (Paterson) road, 13 mi E of Waco, 13½ ft from his lowest layer. Less depth? Possible in good clay. 81 ½ mi S of Zittel & Sons factory is place where they get their clay. 5 ft covered by 2 sand. 82 Enrred frm Cottage Hill & dam to Fox Hammer handle used for area measurement. 6 ft Gui Den E. partly exposed 3 ft 6 in Blue bedded limestone check. larger fair. 2 ft 6 in O and, partly exposed Orient Devil's Den unknown, but believed to be about 12 ft 6 in. Not measured; Thin limant mes and clay. 1 ft fern E. overlaid 3 ft. clay. 6 in clay, muleady, & no farming in mo., 3 in clay, overlaid 1 ft topsoil = mykthide and Brady's Ridge. clay. Top bed with many larcorn. 5 ft direct interladder with Green marble. 6½ ft earth rather massive, 3½ ft down to Stephs muleady. 8½ ft again to Steghs calcarean. 53 ft down to ventral side of Hamphiremena, &y proter in half. But no C or L oh any. Slate's unknown but of pla- minning a retorta group. several of otherative authority to me > 92½ ft Blue Clinto.

(49) 83. Valley View. Othis borealis and chesty gasteropods neat hard fly at eastern edge of turn. Fine exposures of Catheys for 2 miles further east. 84. Tunnel 1 mi NW J William: Strophomena halliana at west end of tunnel and stroph. like fluctua near turn, about 1/2 mi E of William part of bridge 62. 85. Strp. halliana commun, W RR cut. 86 4mi W J Richmond + 3 mi E of William, Ry Stretch. Planor- convexa. J. M. Schiarbrough

276 At Whites station dark clay s.l. Platystraphia lynx at track level immediate south of statin. Dip 2 ft in 100 ft to north. Filled by shale. Then by more dark the clay divided with Platystrophia lynx. The Wp of last named arch is some 25 ft above Whites station, Thin brown shales, 45 ft to base of Clinton. Clinton here according to this is stratigra-phi cally 45 ft above Beds carrying Platystrophia lynx, Clinton. 2ft 2in Massive led at face 7ft Clinton heavy thin lime layers interbedded with clay 4 ft 1/8 in, chiefly clay but with rather ammeous clay eg. rock layer - 5 ft clay bed further NE near Panlato, large crinoid trades of Plat- istrella about 1 ft below base of the 5 ft clay layers. The clay layer is getting some calcareous towards SW, 7ft limestone, but interbedded with considerably clay, 21/2 ft li assigned to Clinton Topmost layer believed to contain Shuck endinum specimens per n, 2 in. Layer with pink ochr Earthy bed at face of black shale the 51 This 15 in. of limestone lie north the Fish tooth layer can tain much calcite in some place, in great latches. The way be rich at lower part of Dernnian below fish layer at Elliston road work 275. RR crossing over cracks. Dipping slight here. 11 ft Clinton to base of clay bed, 18 ft to top of limestone layers rather frequent. 10 ft Bedford clay, So it is interpolated from Paula section, in the be- lief that the strong south- ward dip is about here. At any rate the dip at the Dernnian exposure 43 mi. 5 275 is small, 2ft. My be massive bed in Gasper See Osmine section to Weather sandy form. 2ft 4in' Fine fish plate at base of this layer, same as at Ludion Fields. K. Also Black nodules.

1000 Berea 7 AM. 87. J.C. Baker's farm, 3 mis of Ringtn, 970 ft. 8 AM. 5 mils of house. No exposures at me here. Siltfieldella bed. No fossils. 3'2" top of heavy layer at top of 7'ft massive Clinton limes. Fault with Dermin on N on same level as Clint, on S. North of J.C. Baker house. Strong plant toward SW, Section not well expressed. 6'2" gray Derminian l. 1'ft limestone, weathering chalky, fish layer, then, at top, At least wit very small inodular material. 88. 1/2 mi. NE of New Liberty church colored and 1/2 mil S of Robtann store, There is a layered section of soil overlying the Black Slate west of the road corners which is probably the equivalent to the clay at Jane's Grove section, must be at this layer only. Derminian at junction of roads and also 1/2 mi. W. reduced to about 1/2 inch sandy layer equivalent to fish layers, 90 89. N. of Dave Garrett's house at N. end of Bobtann. Der. limestone at least 4 feet thick, me sees as five layers. Total not less now. Exposure poor. Fault here. Ordovician on same level or north as Dermin limestone on south of fault. I made a mistake here. In the well at Joe Creek Kump's downse the Black Slate rests or nearly directly in the Oford beds that over intercedeiate layers of Derminian were found. Probably this is only a little fish layer here and the rock at Dave Garrett's is Clinton on, 1020 ft at 9.45 AM. The distance from base of Clinton at Dave Garrett's to base of Black Slate at Joe Creek Kump's is 16'ft. There may be a contact cut right here. They weren't 13'ft below Black Slate in well without reaching massive Clinton. at Mat Morris property, honeers is Der. l. under Black Slate & in shale. Oxford clay below + Black Slate about. Farther SE than Der. l. is 14 mi. thick at crossing wn stream.

91. At end of Jackson hollow, about 1 mi SE of Boston, Earthy beds of Black Slate. 9 in, Der. l. 11ft chiefly clay with thorns to included in lower parts. 9 in limestone 5ft chiefly clay, very little else. 14ft. Thin of or rather thick layers of limestone with clay & clay beneath, 10ft to top red sandy layer with white fiddella crumma. Days crimson leady crumma about 14ft below top. 8ft. Massive Chint in lace. 92, at Mathrroys dunel & strm, Black slate. 16 in. greyish argil. 10 in very chiefly Der. l. 10 in. grey. a little chalk. 16 in. greyish Der. l. 12 in. Reddish laminated Argout 12 in. reddish lamin. Gypsum. 5 ft of Der. estimated at 43 feet above top of massive Chint & l. 870 feet at 12:30 92. S of Log Cabin school house, Fault line. 6ft trip to bare clay section. 8ft 4 in. Massive Chinta. 52 ft Ordovician. Dermium absent? 93. North side gully of Grand Creek, at base Black shale, 4ft clay with layers, Dermian absent. 8 in. l. believed to be Gypsum, 12ft Gypsum clay. middle limestone. Further N. there is a fault with Black shale on S and Ordovician on north. 94 S of for Smith. White Gypsum shale. clay 2 1/2 ft trip to hard clay argil in Black thin Black shale. 6 in candy Der. Argil. Gypsum clay. 95 On road going E (white) H- Black Slate on Gypsum l., 3 inches Ordovician clay.

96 On road going E, SE side of valley 4 ft. top of white clay rock in B.S. this [illegible] Black Shale, 2 m. Der.l., Fish scale. 14 m. [illegible]. reddish hmm. 10 ft. [illegible] clay, stream bed. The rock above the fish tooth larger away is equivalent to some of the Der. beds claced with Der. l. elsewhere. There are some clayey beds in Black shale further up which are probably the clay beds elsewhere. 97 Bear Wall m., 995 ft at 2,450 M. White [illegible] Clay with fern [illegible] sandy stuff in it. Bottom well 1060 ft. N.gtonm, 293 D E of Locality 273. Rocky Fork. Black Shale beads + Cyathiphyllid crabs. 5 1/2 ft. brecciated layer with crushed 3 ft. l. with coarse chert. 3 1/2 ft. grey l. very little chat, 6 in. [illegible] Der.l. Rocks much broken + section difficult. A short distance west is a clear section of 11 1/2 ft. Devonian l. a few ft are 1 ft layer of massive Be- good limestone. 23 ft beneath Devonian not well exposed. 10 ft. Several heavy beds of limestone at top of sec- tion. Coarse limestone one wedging the layer with large crumbly beads. Lower part of [illegible] + Chint m. not in shape to measure here.

272. Chas Baker, Wasm Fork. Black slate. 4 in. dark gray clay slipe. 1 ft very cherty. 4 ft very cherty rock like the immediately b. in appearance, July 12 ft of Devonian exposed further south. On Beesford + Clinton section see other book. Sections 272 & 273 should be interfered in light of White’s station sections - 5 ft¹ clay lid partially unimmediates below the heavy layers of lime stone between 74-10 feet above over arch. L. layer above Cervoidal lid at 273. 271. Phosphatic nodules 1-2 inch long. 102 ft = measured section of Black slate. Dip unknown + real thick ness therefore unknown. 11 ft Devonian resting on coral limestone. 269. Der. l., thick, about as thick as 271. judging by eye. 98. Considerable Der. l., too much broken down by weathering to meas. one. Much cherty. 99. Headwaters of Harrim creek. 3½ mi. W. Canterville. Black shale Black shale agg. immediated lagu films to 1 ft below Dp separating two streaks of black shale stuff crecitated at top. Thin 7ft Der. l. like reccaled layer 4 layers like clay weathered back, a streak seems not to soft to have 5½ ft practically not exposed. Shrunken shaley 4½ ft thick clay slipe mottled 37 feet Beesford clay fairly well exposed, 15 inch. masses in Des. l. 10ft chiefly clay

271. E of Cartersville which are mine certain, hand wit sections note it should be cun- since this is only an ext. 19ft as a guess to top of Copad. perfectly clayed above. 4 ft cement + clay interlaiden. 14 ft face of Clint on to top of sandy layer with White feld della olmand out. Much white Divine Clay 2m from Cantersville to Wallace ten hit the Der. & Clintm exposures are fern. 100. 1½ mi E of Wallace ten sulphate mudules? 85 ft measured thickness, ? sh. (only 4 ft of Devonian seen) hole, filled with mud. Laserto Black Shale. 35 ft from large crey spot. 12 ft Clintm face to top of large felds? Large beads. Bear Rusk section-½ p (see next page. see next page. thi frm in army to Bear Rusk 11½ not exposed, covered over before trench + clayey. 4 ft bont and limost me neatly 6 inches are greenish. 3ft soft clay, fret me. upper 3ft freest me in several layers. 3ft good arid, freest me. shaly. 0m freest me, same pit pon + 29½ thin shaly Wardsly. gate (Bear Rusk) 16½thin grey shale, to level of [large spinifera?] [as a ledge. Cantz & ali. Hard shaly clay arch, remain shaly Wardsly, perages containing crinoid in large urdian shaped section. freest me also occur only at top in fossil forms both ext + crave shale, Wa shaly, faintly, Cartersville. 2ft parallel irregular grey thin grey shale Wardsly (23) changed Wardsly bl. ale shaly soft grey stuff, de- [day Blue Fish clay] Hard to meee. made a layer in part of Gilbert Black Shale.

101 continued. Top of Berea Hills fossiliferous, as below (675) 19 ½ ft came sandstone after 30 ft not exposed coal measure part = 21" somewhat fossiliferous (625 ½) 83 ½ ft (brown sandstone after 10 ft limestone in sill, (542) 1st me. (532) 7 ½ [white] crystalline lime- fossilizing limestone 460 ½ fossile this hold erratic mm up to here, a rather 38 ½ f[ing]est me experiences cm. of this section, (422) cut abundantly in lower half two levels. corals weathered 38 ft limestone exposed at number- 12 ft limestone ledges I distinct limestone. 14 ft [white] limestone. first very 4 ½ ft soft clayey shale. 2 ½ ft just one layer in several beds 5 ½ ft soft shale (varied) glaucon making part of it sandy with distinct white quartz 1 ½ ft a sort of firm hard freestone 4 ft not exposed 1 ft pure limestone. 102. Berea College brickyard. (63) G.I and Automatic, Brick maker made by Jonathan Creager Sons Cr. Cincinnati, O. Standard of models, made by the Willington ma- chine Cr. Wellington, Ohio. 601. Strip spoil about 3 inches. Clay used: 3 ½-4 ft. use a track car and cars haul clay from pit to incline by line, 5 up, incline by steam, using cable, at top of incline day is dumped from car on to plat- form & shovelled into disinte- grate consisting two large steel rolls between clay passes, and any pebbles are ground to small size. Water is added to clay as it reaches the rolls in disintegrator. Clay drops from disintegrator great a into pug mill made in Cincinnati (here revolving blades mix the clay and if necessary more water is added. The blades push the clay for- ward into the brick mull, The blade in brick mill press the clay down into the arms.

of the brick mill and these arms push the clay side wise under the press. Here the press punch the clay into the mold, Nine molds when machine is in operation. 6 bricks are made at a time in each mold. Here a man clears the mold and brings it to right and left as necessary to loosen the clay in the mold. Another man fetches up mold, puts it on the turn table revolving wheel, places its side against pallet board, clamps the molds and gives brick in pallet board. Then to put mold in order, Here the mold is pushed thru the sand, And on the other a man picked up the mold & puts it once more in the machine. The sand is clean fine Cincinnati fine. white. 9 pallet boards with bricks are traded on truck, and then they are wheeled to rack. They stay there off by about 5 or 6 racks, th day. between 6-9 days. Next to are set up in the kilm, and a fire made on the 4-5 days. Onest red heat 3-4 days, while (65) treat 3/2, 4, days, Takes 8 day to cool. I have 3 kilns 225,000 brick, 200,000 " 200,000 " Capacity of yards 2,000 red bricks a year, if worked to full extent. in operation 3 years ago. Have machinery for making tilings, but none made yet. Racks loan some for 120,000 bricks at one time = drying racks. 1. W. draft kiln. Morrison draft clamp. 2. Common up draft kils. Clay was Black Shale. Prof. S. C. Warren Korea, Ky. Agriculture, Geology.

103/1 min N of Pout Lick, 4 ft clay, limestone, lynx. 8 ft clay shale, var fossils. 24 ft Orthorynculus? Comm. & lim 5 ½ ft Bryozona collected, lynx. [illegible] limestone, shaly limestone and 10 ft Limestone + Pl. Lynx. 9 ft up: St. mag., big foot/Comma near top? 6 ft. at top: one large St. magnillensis 5c in vexc = magnillensis small? 7 ½ ft. at top is an allophite St. plauer. 2 ft. Strophomena magnillensis comm. 15½ ft Stroph. magnillensis comm. min. at various levels. 16½ ft. Str. magnillensis comm. funn. at various levels. James had cut of lynx recurs about 2 ½ ft above line of this tick, a short distance NW a fence line. Here limestone runs into m. crosa traded 2 andy rocks top of O garard & and stone, but the St. magnillensis extend 6½ ft lower down, cut are I may go down further 66 ft O garard so I down as far as creek, but have not seen. Rafinequeam + C in l. beds at various levels. 104. East of Wallace mi 2 ½ 15 ½ 93 ½ 9 102 ½ 2 ft. 9 in., in 30 slabs 30) 9, 70 (30. 94 12) 270 (22 30 82 ¾

1/2 ac W. S Hammack 69 105, about 4 mi N of Flat Worm Church, Devonian partly exposed. Ac- cording to estimate at least 13 ft thick; the upper object corresponding to the visited layer, and the lower 7 1/2 ft very dirty. At least 20 lb of Oxford clay according to estimate, there being considerable clay accord- ing to stuff brought up in sand hirlers and by clay fish. No good experience. 106 11 1/2 by upper Oxford clay exposed, [but] about 6 or 7 soft 15 mi. Layer L = original big layer, 11 ft not exposed clay, apparently at least 30 ft seen. 1 ft layer L.

107. Peter Spain hovers is correct on east side of branch on main Lancaster road, west of home of Peter Spanhanger. This line is an east side hand. Line Der. chert fragment have been 44 ft.) = Besard clay, thus may 33 ft w't. clay exposed at by 52 ft massive Clinton. Barny Clinton. Contact w't. greenish slaty bedded cam. 108. Lauza Chapel, 109. Fall Yick & Lancaster pike, br /Hammack, James M. Anderson, Black Slate. 52 ft Derivianal brecciated fa siliceous 5 1/2 ft clay chert. Base not exposed. 22 ft Besford clay, to base of 15 inch heavy limestone 58 ft chiefly clay; 27 1 ft heavy limestone large, 3 ft clay my limestone & clay, large crinoid beds 1/4 fin. thk. 3 ft [illegible] markedly more heavy layers 7 ft massive Clinton, Arthur lynx occurs 1 mi further west just east of main cl way over Gilbert creek.

May 27-31 July 16-18 July 30-Aug, 20 service (5 days) 110 James F. Harris, NJ Drive, My Estel Springs 4 mi. across creek wt. built side. +7½ 3 ft clay collected. Sandy shale fragment much less abundant here, sand toward -½ 11 ft small shale fragments in boggy clay, 16½ ft considerable sandy shell bed good. 2 ft massive limest in boggy. Along road towards Estel Springs from Harris, Fossiliferous over the 2 ft massive limestone in boggy. Chiefly on about the range 16 feet and at the top is a hygroma layer with in many fernsillodot or fine black flint in extraord, and a white bit of intercalate marl in my free check. Clay collected from 2-13 feet be low the 2 ft massive limestone bed. The section 0-2 feet below 2 ft marlin bed not observed. Below this lower clay is thin limestone intercalated with clay in great quantity, 12 ft. The mixture well exposed. Possibly the 5 ft clay bed be neath but not well exposed.

(Black shale shal 112. N of Waco. 6 in soft clay rock. and clay arch in middle part (75) 7 2 ft 1/2 in hard clink at top Black shale. 3 ft 9 in Dorseyville No chert. 19 ft upper clay, 2 ft massive bed, 12 ft chiefly clay, 8 2ft chiefly clay, 5 ft chiefly clay. 4 ft streak to top of Whitfieldella bed. Mr. Jesse Jones at Union Hall, knew all about the fire clay used to be kept keepers at the furnaces & furns where fine clay was obtained. At Union Hall was formerly the Cottage Furnace. Pitching Furnace on Miller's creek. Estill Furnace on dividing ridge between Hardinckle's creek & Miller's creek. Cottage Furnace, on dividing ridge between Ballard Forking Hardinckles creek & Cox creek = or between Cottage Fork & Combs Branch. Sam Ginter at Union Hall, G. W. Lyle at Vaughns Mill, for information Estill Furnace of Sandola 45 ft clay top not near, 7 ft with lizzie to top clay &. 2 ft massive cl, in Oxford. 12 2 ft clay 20ft top of grl'd chintm to by a middle limestone in clay. The 5 ft clay layer from brow 5 ft & this section clay collect

258 at Bill Mankes house 1/4 mi. E of Crab Orchard station, Cyatophyllum crals. D. phyphyllum [illegible] Farnites handlings fairly Lamellos. Cladifera? 12 1/2 ft of Pennv'an exposed the top 1/2 ft is less fresh stems but the remain- der of the section contain many crals + a few branchyferda. Not in a con- dition to collect. Many could be recognized if Davi's crals were taken into the field. Apparently the upper 1/2 foot of section just described which may equal 3 feet when fully exposed equals the brecciated layer. Base of section not seen yet. 11/3 At Mr. Howard's lander, About 1 mi E of Bill Mankes small spirifels are seen on surface of grey Lynn layers. Being siderolite both for identification. About 3 feet of Pennv'an exposed. Brady Myoda from 0-4 ft above bed. Not critical. [77] Markings cloud seem very critical all are abundant immediately above the bre- ciated layer. 114 E of Crab Orchard, a road across Dicks river. NE from Bill Mankes, 3/4 mile. Black slate. 11 ft Derv L in Layer 1-2 ft thick. Crals at top. Not critical. Concentric. Blotrophyphy lons. 4 1/2 ft. Der. L. at tip one large spirifus + crals. Berry barks. Not critical. Large styfra reticularis. 33 ft Beyond clay, Hastiliforms, gangers are massive 2 foot bed not seen. 248. Immediately N of RR W of Crab Orchard, sand layer but amount part equivalent to free- 11/2 ft Derv L. crals at top upper 5/8 ft Farnites + dark grey spir.d. 3 1/4 white oil, eroded at whe weathered. Rather E a more directly vertical section measures 18 ft.

(79 256. Byrn, N of Crab Orchard, Black Slate. 12 ft Devil, oz ath oply slud end + Blithing plyllum not well preserved. Bym beds healthy red with brim except top 4 in our which are decorated grey, From 257. Dixie crossing, towards 256, Dev Limestone. 65 ft of clay black well exposed face not seen. Massive bed overlying lower Brum Middle clay not exposed. 11ft to level of bridge. 5 ft limestone alternating with clay rock especially along middle corresponding to 5X clay layer. Slu tip 10 in = solid limestone also the bottom 8 in = 2 layers cold lime. 14 ft successive limestone, Large crinoid heads + what ? shells islands looking limestone. Going N a large mass of limestone slat, presumably the 2 ft layer, lies 10 ft above the level of the bridge. From far it has dropped form in situ to incline. 39 ft above the bridge, by min N of the bridge, where the steeper part of level begins, the 2 latter layers will be seen to dip towards the south. On North of hill going down towards Drake creek, large successive specimens of columnar varia's halls are common; according to my calcs allows they join 75 feet below. Chatham at least but there is a fault nearby at least. At this fault the large beds on south have dropped, dip is South. Plenty strophosic layers extend at least 25-40 above Drake creek at N side. About in accordance to level of 70 feet higher my last club undermined + fault. Under to present level along my line, Black Slate 3/4 mls NE of Swine.

120. Mine fault crosses western margin of Richmond sheet on north side is only about 1/4 of Rich- mond and in the good Harmonme section from to Duck Creek, on south side is Christm with part beyond, then fault and deviation low with black slate in south side of second fault. Further north Kinder is brought up by fault on south side in a larger level than Dec. 1, in the middle. 121. S mill. of Harmon creek with Richmond + Chat Orchard and. 5 ft thin l. s clay. 6, sand l., bed at top 8 in thick, intercalated in next one, 5 1/2 A emeri decent clay with 12ft massive limestone, 11ft from lower Clinton exposed to top of layer with large chertic leads 3 3/4 yesterday, look at 11 ft with shale this forms the [illegible] 1 ft limestone in mass. 5 ft cherty clay 344. 2 1/2 mmi. west y Chat orch ard) along RR, 16 ft Dec. 1. some of it which has grey earthy. 5 act well SW of line. 320 Cedar Creek, 3 miles west y Crab Orchard, Sudden dip S in north y em. prome, m mile Ethern. 28o 35o 3 ft up is top y another l. layer. 8 in studdy massive l. layers, 5 1/2 ft. partly exposed = 5 ft clay ? 2 ft massive 2 or dry l. Large windblow 2 ft Lemat exposed 2 ft? 2 ft massive l. 2 sand at top 17th. partly exposed soft ? 3ft 4 in, massive layers. 4ft 4in massive l. Clinton and mican 249 just NW y Walnut Plate), about to me. Large chertic leads in Clinton on (or) W of and NE of prod a overlym rock exposed story with smutt The stories of Clinton at least 6 ft but surface area of telling cored the worse, faulting? Massive part only exposed.

At Sweeny Mynars. Divina lines in dis- inct. Devonian line also at Morris at mouth of Red River also west of Stanford at reservoirs. 250. 3/4 mi. SE of Walnut Flats, Clinton more than 100 feet above extreme at 249. 122 NW of Cedar Creek Crossing of dike. 1 ft massive layer 3 1/2 ft after 10 ft Clinton 70 ft Ordovician No. Lynx, 122: 70 ft Ordovician see note above. 233 East along pine grove turning N from pike E of Cedar Creek red shale with Dac crabs. 66 ft Bedford clay at 2 ft beds 15 m. Massive l, = 2 ft layer? 6 1/2 ft chalky clay Almost 2 or 3 commixture of several layers.

(85 Strine formation along creek road about 10 feet above cam fan and for some distance upward, going west 123. Along road following east side of Cedar creek north, 50 ft. up to farm of Clinton. 37½ ft at top & Detradium, (chalky). The same formation with lync, Overlying a fault beyond (Colum) Detradium layers? 259. NE y Crab Orchard 9 ft Dev limestone, 247. On Road from Crab Orchard to Chapel Hill. 11 ft Dev limestone, 246. Head of Cedar Creek: Wyler Expire clay apparently at least 50 ft thick. Not well exposed. 245 West of Cedar Creek on county road, Now solid limestone, about 3½ feet, not well exposed 8½ ft Clinton, 124. Western branch of Cedar creek where county road & of R R crossed at Abel Brigant's home red soil with Dev Trachypods. 35 ft Upper Oyster clay, 2 ft layer massive limestone. 6ft middle oyster clay 2ft Chaffy cl. with interbedded clay. 1½ ft partly exposed 8 in. solid, cl. 5 ft partly exposed. 12 ft base to top of chert in large crushed beds about 2 ft below trip, Continuation of successively lower profiles going west! 125 West of same branch of Cedar Creek east of George Bone's home. Dev Trachypods order in secondary clay, red! 8½ ft Devl. NE of house at spring.

126 A short distance W. of 125, Eg creek Den limestone. 20 ft Upper Ceperd clay. 2 ft Limestone massive layer. 5\frac{1}{2}ft Clay; first exposed. 1\frac{3}{4}ft limestone. 6\frac{1}{2}ft drifty clay, 127 At William Pleasants, west of Little Hendro. 6\frac{1}{2} ft at least to Den. [illegible] limestone. 11 ft Upper Ceperd clay. 128 West 1 where a road turns off north on County Road the same as Der. L. (3 ft thick?) is estimated at 6 ft over ridge which may be the massive 2 ft layer. (Wm) James [illegible] Bailey 24[?] Where county road turns NW, Black slate, 1ft red clay - Den. l. \begin{cases} \frac{1}{2}ft clay & 7 belng to 5 ft \\ 4 in claysel & ) clay series \\ \frac{1}{2} ft clay \\ 1\frac{1}{2} ft limestone massive, \\ leads 1 ft Belno Tip. \\ 12 ft to tip of Clinton layers and \\ 40 ft Richmond, base not seen \\ 129 School SE of Wall Gap Station. 100 ft Richmond but no ligny at basal section; hence Richmond is thicken. 241. magnets Black slate apparently faulted against limestone in south where silicim is disintegra- ted into white sand with underlying black slate. 246 Road going N from county road. 12 ft of disintegrated iron till, black slate, schistus, I suppose is [illegible] at least limestone below? 239 Limestone beneath Black Slate Own expense. 130 One third mile NE of Rowland Colmunaria Hall common in road side in front of house. Further north = \begin{cases} 17 ft to next 200m \\ Colunmaria alveolata. \\ 50ft Richmond & below. \\

131. Half a mile E of Rm lands, Columnaria chrumma left side y road. 132. Beyond grad angle when road to Breacherville turn off. Whitfieldella in loose blocks. Some Clinton in place. Plenty of Der. chat above. No room for middle + when Oxford Clay, I think. 133. North of RR along Rrad follow by west side of Cedar Creek, Columnaria albedata com mon. Some are 2 ft across. 235 Brecciated splendidly, 11ft exposed. Faulted against Admontia 134 Black Slate. 6ft Der.l exposed. Total underway. 135 Much cardinal Der. chert on top here. Contact between Black slate & lower grades not seen to mi S where it should be. 233. East of Cheese Factory. Lance Black slate. (Katie Adols) 4 1/2 ft Der.l, probably the total. 27 ft clay shale. Platystrophus lyons & gaster pres. Great fault, sides in S side have dropped. 131-132 East of Rm lands along pike. 1000 RR crossing. 1022 Columnaria 1095 95 ft to base of Clinton 450 times washed. 1028 Columnaria's 996 RR crossing 95ft - 20.4ft = 75 ft splenic matey, possibly a little less. 22) 450 (20.4 ft) 442

136. One mile N of RR along Logan Creek, Yelarena illemlridala. Heteropemya, in upper lynx bed. [illegible] 137. On S side of branch 2 mi's N of RR at Richland, along west side of Logan Creek. Platystrudalia lynx bed, blue clay; typical lynx shale, on S side of branch, about 10 ft above creek. Richland & E thickness of Richland, Base Clinton. . .75 ft Columnarales. . .50 ft. base of section 136) Total = 125 ft and lynx beds not seen. 201. Blue Slate, NW J Simmietta spgo. at Junction City, Phosphata nodules common, Many 3 in. long, a few 4 inch in length. level, have dipped from higher areas here but they are very Broken mainly shale frag- nodules at top =86 ft thick mixture of ferruginous phatic on uncertainty the which I have called film- 25 ft clay, nodules at top stretch. nodules gone at top of this 11 ft clay. The same phosphates (1 inch) line at this level, 31 ft clay, phosphatic nodules this level diameter within 1 ft above Phosphatic's modules 1 inch in 11 1/4 clay 8 in ferrug layer at top. 9 1/2 ft clay 3-4 in ferrug layer at top, nodule layer with abundant modules common or at 4 in. above top of Black slate rare up to 2 1/2 above Black slate,

260 Doniphon's Cut My Junction City Incipient markings will developed as at Chat Orchard, Spring fin hiatos as at Chat Orchard. [illegible] [illegible] Plat: lynx, Base of Daniels. 7 ft clay grade cracking up useful only. Rapid lynx circle with > fossils listed above. 4ft s in dense whitish l.+chat 6 in. dense fluid white l. 2/8 4in. dense fleckish white l. 4 in. badly weathered l. w/th pss? 2 ft. White dense l. 2 ft 6 in. dense light gray l. 93 Fishing Creek, E side. Higher up, July. Rattler rare for 2 ft. Nodules chiefly at base Wa. Fossils collected up to 25 ft above face of quarry. Nodules up to 3 or 4 inches. Large crinoid bead common. 13 ft above face Clinton. L.F. Shadow, at Spring below first trowee level I might ride if creek then is 7 ft. of Chinta over 8 ft. wide which looks like massive Andersonian (Anderson?) Below is after this rock breaking up irregularly. About 3/4 mi. above the bridge.

Sulphur mill, 1 mi. N of Columbia road crossing on Fishing Creek. Black slate, 6 in chert layer. Cavities resembles fish bone, with ripples & subfossatic black 2 ft 6 in. Der. rock Black jasp. [illegible] after regarded as Gerd. 1 1/2 ft Cherty clay ferric clay and micaum with ? T. P. Jasper, about 2 miles across east to Columbia road crossing, and 2 mi NW, or east of Columbia road. Chert & chals in Der. Farther north, 1/2 mi. On Der, 2 sandstone, 2 ft thick, sets my Gypsa limestone & clays much intercalated. Determined by such ferrum crlm ulmig, 1/2 large crithria leads founds on good section about 8 ft thick, at next house or middle of creek going W there is some chert over 4 ft of Der. with my chert. Farther north, south of 2 our mill & linnse is Black slate 2 1/2 ft Der. see the b. without chert. no any anals, 3 1/2 ft cherty cl. face not seen. Black slate 4 in. chert. 5 1/2 ft. Cherty Der.l. spids come mm at tip. Mr Taylor Brock. Black slate | Best place for 5 in. Der. l. fossils since long 5 in. chert. by S branch of 3 1/2 ft Cherty, Columbia pete. 3 1/2 ft massive sandstone or denzel the accede character not constant arm at once experiment, = complete Der. section my large crasse Septaria Mimbidalis phacips fast, Dalmantes barb Amiba var. y fossils here above Machi Ardo.

Further N. 200 yds. is N. bank of Columbia road, here the massive rock is fully exposed just below the chute, middle section of Denning. On N. side of Columbia road half a mile east of Clifty creek at crossing on Clifty creek. 8 in Banktown rock, Bl. Slate, my. 1 ft Devil's chert 6 in. chert 4 ft 3 in. clifty Den 3 ft massive D. Den Beyond town rock. Rogers Gap. Lower part of lower Utica but not lowest part. Contains 2 specimens of Crepispora verrucata, Helcero- trypa present. Ladysville, Middle Utica. Indian Fields is Madison bed, Hemotrypa Minutifella quadrata Bathstoma variabile Hemotrypa flabellaria. William, west of Richmond. west end of Tunnel to Lava & Middle Utica east end of Tunnel = Middle Utica west of bridge 62 a shelt Distance east of William = Middle Utic Locality 44 next to Indian Fields at mile post 30 east of Lexington, Mt Auburn Gymn. Sch. Loc. 49, James Hornback, west of Indian Fields, little gully N.W. R.R. = Mt Auburn. Loc. 62, Merritt's Ferry, have little dust from Gymn. Beds - Mt Aubu Amphedra schizotifera = character

99

Go to Hurst, turn to left (SE) about 1/4 mile, next on pike

Winchester 1160 Run to depot. 955 L+ E Junction 1110 995 Gordon 1170 910 Indian Fields 965 915 West Bend 935 830 (Argyle) Viridian 880 790 Shawnee 850 Clay City 845 Stanton 865 Cat Creek 870 Richmond 1020 Whites 970 Chilham 930 Carterville Richmond 116 9 Mobley 1120 Muddy Cr. Brassfield 1000 Purila 912 Kings 910 Rice 838 W. Irvine 790 Irvine Turn 790 Berea 1000 Childers 990 Whites 982 Inch'n 1050 Richmond 980

Univ. 850 Cincinnati 432 Ludlow 535 Erlanger Richmond 924 Walton 912 Braclet 919 Crittenden 908 Sheridan 924 Dry Ridge 949 Williamston 743 Main 924 Blanchett 953 Erwinth 953 Hinton 943 Sadronville 857 Rogers Gap 913 Binkard 862 Gorgeton SR 864 Denmark 882 Greendale 942 Lexington 960 Nicholasville 946 Jessamine 886 Wilmore 872 High Bridge 762 Burgin 887 Danville 955 Junction City 982 Murland 1086 McKissney 1008 South Fork 976 King Post 1168 Somerset 867 Burnside 708 Butler 604 Falmouth ?530 ½ Paris 826 Winchester 1160 ½ Richmond 926 Harris 1009 Silver Creek 809 Lovell 799 St George 884 Hyattsville 1004 Ganviter 999 Gillbets Ch 830 Stanford 921 Halls Gap 993 Coalbankand 919 Mt Sterling 934 Evington 992 Stephensme 777 Olympia 751 ?Preston 742 Salt Lick 656 Farmer 668 Morehead 712 Myers 613 Carvan 922 Mayesville 508

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